基于计算流体力学的寒区土壤水热耦合模型研究
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Simulating thermo-hydrologic processes in cold region soil system: a computational fluid dynamics study
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图14. 在冻结开始后1、3、6、12、24小时的温度(a)和液态水饱和度(b)的演变 |
Fig.14. Evolution of temperature (a) and liquid water saturation (b) at 1, 3, 6, 12 and 24 h after freezing started |
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